Effects of oceanic tides on tidal variations of gravity at Kyoto and Mizusawa, in Japan, were estimated for two principal semidiurnal constituents, M
2 and S
2. In the estimation, tidal charts newly drawn by the present authors were used for the seas adjacent to Japan. For the global ocean, three and two models were employed for M
2 and S2 constituents, respectively. As for M
2 constituent, estimated values of the oceanic effect change mainly with the global tidal model employed. This suggests an incompleteness of the global tidal models. As for S
2 constituent, it will be necessary to take meteorological disturbances and atmospheric tides in more detail as well as the oceanic effect into consideration, for the further discussion.
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